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The characteristics of minerals, including their solid state, formation by inorganic processes, and specific crystal structures. It also covers the identification of minerals based on physical properties such as color, luster, crystal shape, cleavage, hardness, and density. Examples of minerals and their chemical formulas, as well as the concept of atomic substitution. It also explains the importance of mineral abundance in the earth's crust.
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What is a mineral? The five characteristics required in order for a compound to be a mineral are:
General Chemical Formula Minerals always have a generally consistent chemical formula, so atoms are always present in very specific ratios. Is glass a mineral? _______ Explanation: ___________________________________________________________ Which sample can we eliminate that is a naturally formed type of glass? ____________ Chemical formulae may be:
Two similar-sized and similar-charged ions that often substitute for each other in minerals are _________ and __________. Example of atomic substitution: Olivine - (Mg, Fe) 2 SiO 4 In olivine, there will always be two atoms of either Mg or Fe (or one of each) for every one Si atom and every four O atoms. Characteristic Crystal Structure The atoms in a mineral are organized into regular, repetitive geometric patterns in three dimensions, called a __________________. We therefore say that all minerals are __________________. The crystal structure of any mineral is a unique characteristic of that mineral.
For what type of minerals do we find the streak? ________________________ Luster: Luster refers to how a mineral surface reflects light. The two types of luster are ________________ and ___________________. Crystal Shape: The planar surfaces on the outside of a crystal are called _________________. The angles between different faces are called _______________________, and they are always constant for any particular mineral. Cleavage: What are cleavage planes? ____________________________________________ Do not confuse cleavage planes with crystal faces. They look very similar, but only the very outside edges of a crystal are crystal faces, but there are many potential cleavage planes inside the mineral along which the crystal may break apart. The angles between different cleavage planes inside a crystal are always constant for a particular mineral. This is why cleavage is such a useful way of identifying a mineral. Do ALL mineral crystals have cleavage planes? ________ What are the curved fracture surface in minerals without cleavage planes?
Hardness: Hardness is how easy it is to scratch the mineral. The strength of the atomic bonds controls hardness.
What scale do we use to identify mineral hardness? : ________________________ The softest known mineral is: ___________ The hardest known mineral is: _____________ Density or Specific Gravity: This is the mass per unit volume (different for different minerals). __________ minerals tend to have the highest specific gravities. Other Properties Halite (table salt): ___________________________ Talc: _____________________________ Magnetite: __________________________ FINAL QUESTION: What happens to calcite when hydrochloric acid is spilled on it?